Skip to Main Content
Article navigation

The main objective of this paper was to develop a fundamental understanding of oil sand tailings for centrifuge dewatering. Laboratory characterisation indicated that the investigated tailings were a fine-grained material (53% clay fraction) with a moderate water adsorption capacity (ωl = 55% andωp = 25%). The solids consisted of 55% quartz and 40% clay minerals and showed a specific surface area of 43 m2/g and a cation exchange capacity of 29 cmol(+)/kg. Likewise, the pore water (pH = 8·15, EC = 3280 µS/cm and ZP = −46 mV) was dominated by Na+ (776 mg/L), HCO3 (679 mg/L), Cl (518 mg/L) andSO42(377 mg/L). Centrifugation physically improved tailings dewatering through particle segregation, assemblage formation and flow channeling. For a g factor of up to 2550 g, the released water increased by 4·7%, the entrapped water decreased by 30% and the sediment solids content increased by 7%: all quantities compared to self-weight settling. The corresponding decrease in physicochemical properties confirmed aggregate formation and an effective capture of clay particles in the suspension zone.

You do not currently have access to this content.
Don't already have an account? Register

Purchased this content as a guest? Enter your email address to restore access.

Please enter valid email address.
Email address must be 94 characters or fewer.
Pay-Per-View Access
$39.00
Rental

or Create an Account

Close Modal
Close Modal